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1. Identity statement
Reference TypeePrint (Electronic Source)
Sitemtc-m16c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/ePrint@80/2006/08.08.20.50
Last Update2006:08.08.20.50.29 (UTC) administrator
Metadata Repositorysid.inpe.br/ePrint@80/2006/08.08.20.50.25
Metadata Last Update2018:06.04.04.22.29 (UTC) administrator
Citation KeyPazRoss::PeGyFa
TitlePetrography of gypsum-bearing facies of the codó formation (late aptian), northern brazil
Last Update Date2006-08-09
Access Date2024, May 18
Type of MediumOn-line
Secondary TypePRE PI
Number of Files1
Size244 KiB
2. Context
Author1 Paz, Jackson Douglas Silva
2 Rossetti, Dilce de Fátima
Resume Identifier1
2 8JMKD3MGP5W/3C9JGTQ
Group1
2 DSR-INPE-MCT-BR
Affiliation1 FUA
2 INPE
e-Mail Addressrossetti@dsr.inpe.br
Alternate PublicationAnais da Academia Brasileira de Ciências
ProducerInstituto Nacional de Pesquisas Espaciais
CitySão José dos Campos
Stage of Alternate Publicationaccepted
History (UTC)2008-04-26 01:40:00 :: rossetti -> administrator ::
2018-06-04 04:22:29 :: administrator -> rossetti ::
3. Content and structure
Is the master or a copy?is the master
Content Stagework-in-progress
Transferable1
Keywordsevaporitos
Aptiano
Bacia Grajaú
petrografia
AbstractAn original and detailed study focusing the petrography of evaporites from the late Aptian deposits exposed in the eastern and southern São Luís-Grajaú Basin is presented herein, with the attempt of distinguishing between primary and secondary evaporites, and reconstructing their post-depositional evolution. Seven evaporites phases were recognized: 1. chevron gypsum; 2. nodular to lensoidal gypsum or anhydrite; 3. fibrous to acicular gypsum; 4. mosaic gypsum; 5. brecciated gypsum or gypsarenite; 6. pseudo-nodular anhydrite or gypsum; and 7. rosettes of gypsum. The three first phases of gypsum display petrographic characteristics that conform to a primary nature. The fibrous to acicular and mosaic gypsum were formed by replacement of primary gypsum, but their origin took place during the eodiagenesis, still under influence of the depositional setting. These gypsum morphologies are closely related to the laminated evaporites, serving to demonstrate that their formation was related to replacements that did not affect the primary sedimentary structures. The pseudo-nodular anhydrite or gypsum seems to have originated by mobilization of sulphate-rich fluids during burial, probably related to halokinesis. The rosettes of gypsum, which intercept all the other gypsum varieties, represent the latest phase of evaporite formation in the study area, resulting from either intrastratal waters or surface waters during weathering.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Petrography of gypsum-bearing...
doc Directory Contentaccess
source Directory Contentthere are no files
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/sid.inpe.br/ePrint@80/2006/08.08.20.50
zipped data URLhttp://urlib.net/zip/sid.inpe.br/ePrint@80/2006/08.08.20.50
LanguageEnglish
Target Filev1.pdf
User Groupadministrator
rossetti
Visibilityshown
Update Permissiontransferred to ePrint update
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 7
Host Collectionsid.inpe.br/mtc-m18@80/2008/03.17.15.17
6. Notes
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7. Description control
e-Mail (login)rossetti
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